A flux gate sensor =93modulates=94 the ambient field. Basically it =93attracts=94 the ambient field in a high permeability core, then satura= tes that core with an auxiliary winding =96 the driver winding -- causing its= permeability to approach that of air, therefore the previous ambient field lines in the core are =93pushed=94 out. If the core is surrounded = by another coil which is magnetically orthogonal to the driving coil =96 the= sense coil -- the sense winding is not coupled magnetically to the drive winding, but the flux from the ambient field that is moving in and out induces voltages in the sense coil. A little thought about this process shows that although the drive coil saturates on a positive and negative drive peaks, the result on the sense coil is that the sensed voltage has gone though two positive peaks, i.e., it is the second harmonic =96 it is= two times the frequency -- of the drive waveform. This is why flux gate magnetometers are often called harmonic modulators. Typically to improve sensitivity, the sense winding is resonated with a capacitor to the second harmonic frequency. The Speake and Precision Navigation magnetometers use another effect. Suppose we take a strip of high permeability metal that is easily saturated (easy saturation is not actually necessary, it just makes the effect easier to use.) Now we wrap a coil around this strip of metal and put it in an oscillator circuit that senses the BEMF in the coil. What happens next is that the BEMF collapses when the strip saturates under the drive current. If this is the signal to reverse the current in the drive coil, then the unbalance in the drive current is the measure of the ambient flux. The Speake and Precision Navigation circuits do one more slight variation. Instead of symmetrically sensing and reversing the drive current, they reset the core in one direction very quickly and only sense the saturation in the opposite direction. The result of this tactic is that the time to saturation varies with the ambient field and since this time is the pulse width of the output, therefore the frequency varies roughly proportional to the ambient field. I=92ve been developing a high accuracy, low cost version of the symmetrical form that can be read out with one of the 24 bit DACs that are now so available with a very stable zero and symmetrical plus and minus sense range. The strip of permalloy or Metglas is free to $0.25. A hint for gathering the strips: save all your anti-theft tags such as on CD=92s from Best Buy and other retailers, and make good friends with your local librarian. A curious thing, I have picked up 20 or 30 the tags in the parking lot of my local Best Buy store. I can only surmise that as people leave the store they instantly rip off the cellophane wrapping, along with the tags, in order to start playing their new CD=92s= on the way home. I can easily pick-up 5 to 10 tags in a single trip to the parking lot. Just look down. Current results on the librarian source strips are a noise floor of about 50 pT peak-to-peak to about 30 Hz not counting ambient hum. It=92s actually capable of about a 1 KHz BW= , but I close it down to keep the 60 HZ pick-up manageable. Probably the anti-theft tags, which use Metglas, will not perform as well as the library permalloy strips since the Metglas in the tags is probably annealed to be highly magnetostrictive. This quality interferes with the noise performance from what I=92ve read. I=92ve haven=92t finished t= he experiments in this area to confirm that. Regards, Charles R. Patton _____________________________________________________________________ Public Seismic Network Mailing List (PSN-L)
Larry Cochrane <cochrane@..............>